新疆南天山盲起苏晚石炭世侵入岩的确定及对南天山洋盆闭合时限的限定

朱志新, 李锦轶, 董连慧, 张晓帆, 胡建卫, 王克卓. 新疆南天山盲起苏晚石炭世侵入岩的确定及对南天山洋盆闭合时限的限定[J]. 岩石学报, 2008, 24(12): 2761-2766.
引用本文: 朱志新, 李锦轶, 董连慧, 张晓帆, 胡建卫, 王克卓. 新疆南天山盲起苏晚石炭世侵入岩的确定及对南天山洋盆闭合时限的限定[J]. 岩石学报, 2008, 24(12): 2761-2766.
ZHU ZhiXing, LI JinYi, DONG LianHui, ZHANG XiaoFan, HU JianWei, WANG KeZhuo. The age determination of Late Carboniferous intrusions in Mangqisu region and its constraints to the closure of oceanic basin in South Tianshan, Xinjiang[J]. Acta Petrologica Sinica, 2008, 24(12): 2761-2766.
Citation: ZHU ZhiXing, LI JinYi, DONG LianHui, ZHANG XiaoFan, HU JianWei, WANG KeZhuo. The age determination of Late Carboniferous intrusions in Mangqisu region and its constraints to the closure of oceanic basin in South Tianshan, Xinjiang[J]. Acta Petrologica Sinica, 2008, 24(12): 2761-2766.

新疆南天山盲起苏晚石炭世侵入岩的确定及对南天山洋盆闭合时限的限定

  • 基金项目:

    “十一五”国家科技支撑计划重点项目(编号2006BAB07B08-2)、973项目(2007CB411306)资助成果

The age determination of Late Carboniferous intrusions in Mangqisu region and its constraints to the closure of oceanic basin in South Tianshan, Xinjiang

  • 南天山额尔宾山中部出露的盲起苏侵入岩主要由花岗闪长岩组成,前人认为是泥盆纪产物,对其中锆石进行SHRIMP定年,获得侵入岩形成年龄296.9±5.4Ma和304.2±11.6Ma。其岩石学具有偏铝和过铝同碰撞花岗岩的特征,结合该带二叠纪后造山花岗岩及其它方面的区域资料,从而提出南天山古生代洋盆的闭合时限为晚石炭世。
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出版历程
收稿日期:  2008-07-23
修回日期:  2008-09-08
刊出日期:  2008-12-31

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